
doi: 10.1007/bf01160136
The dyke-like 1.63 Ga Jaala-Iitti rapakivi complex forms a 25 km long and up to 2 km wide intrusive body at the northwestern margin of the Wiborg rapakivi batholith cutting both the granites of the batholith and the surrounding 1.9 Ga Svecofennian crust. The subvolcanic-epizonal Jaala-Iitti complex consists of silicic (quartz-feldspar porphyry) and basic (diabase) rocks as well as more abundant intermediate hornblende-bearing hybrid rocks.
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